Information gathered on past flood events is essential
for understanding and assessing flood hazards. In this study, we present how
citizen science can help to retrieve this information, particularly in areas
with scarce or no authoritative measurements of past events. The case study
is located in Yeumbeul North (YN), Senegal, where flood impacts represent a
growing concern for the local community. This area lacks authoritative
records on flood extent and water depth as well as information on the chain
of causative factors. We developed a framework using two techniques to
retrieve information on past flood events by involving two groups of
citizens who were present during the floods. The first technique targeted
the part of the citizens' memory that records information on events,
recalled through narratives, whereas the second technique focused on scaling
past flood event intensities using different parts of the witnesses' bodies.
These techniques were used for three events that occurred in 2005, 2009 and
2012. They proved complementary by providing quantitative information on
flood extents and water depths and by revealing factors that may have
contributed to all three flood events.

Together with Asia, Africa is the continent most affected by floods
(UNISDR-CRED, 2015). Between 2000 and 2018, there were 698 flood disasters
in Africa, killing more than 14 250, affecting 45 million people and
causing USD 6.8 million of economic loss (EM-DAT, 2018). West African
countries, such as Burkina Faso or Senegal, appear to be experiencing an
increase in flood disasters due to population growth and the urbanisation of
flood-prone areas (Di Baldassarre et al., 2010). Between 1990 and 2014,
floods were responsible for 86 % of the economic loss from natural
disasters in Senegal alone (Preventionweb, 2018). During that period, the
years 2005, 2009 and 2012 were marked by severe urban floods, particularly
affecting the capital of Senegal, Dakar, causing human casualties and
impairing socioeconomic conditions (GFDRR, 2014). The country is facing
enormous challenges in flood risk management, exacerbated by climate change
(Douglas et al., 2008; Urama and Ozor, 2010), rapid and uncontrolled
urbanisation, a lack of drainage infrastructure, and rapid changes in land use
that worsen drainage patterns (Chen et al., 2015; Ahiablame and Shakya,
2016).

The government and local authorities of Senegal have tried several
strategies to mitigate urban floods, such as developing emergency plans,
relocating inhabitants and building water retention basins. However, two
key aspects, required for these measures to work, have not yet been
considered. First, it is necessary to understand the causes and
characteristics of floods, and, secondly, the local population must be
involved in the process of risk management. Information on the magnitude and
intensity of flood events, as well as on processes controlling the flood, is
at the core of flood hazard assessment and zoning (EXCIMAP, 2007). This
fundamental information is scarcely available in the region (GFDRR, 2014; Sy
et al., 2016). The absence of an organised data acquisition system during
floods has led to the absence of a comprehensive catalogue on past flood
events and consequently on flood hazard maps.

Without records of past events and without the possibility of capturing the
temporal dimension in terms of the frequency of occurrence, accurate flood
hazard assessment is impossible to achieve. Moreover, floods are not only
triggered by natural factors, but they are frequently influenced by man-made
processes (WMO, 2012; DAEC, 2016), which are not easily recorded by
ground-based instruments (Townsend and Walsh, 1998) or remote sensing
(RS; Sanyal and Lu, 2004). Consequently, new alternatives must be explored.
Citizen science is a form of collaborative research involving citizens in
scientific projects (Wiggins and Crowston, 2011). Citizen science has
attracted much attention from scientists in many fields such as ecology
(Dickinson et al., 2010; Silvertown, 2009), astronomy (Raddick et al.,
2007) and more recently hydrology (Buytaert et al., 2014; Paul et al.,
2018). Rapid advancements in various modern technologies – the internet, web
2.0, virtual globe, location-based services, social media, mobile devices,
interactive geo-visualisation interfaces such as OpenStreetMap, Google
Earth and Geo-Wiki (Fritz et al., 2009; Mooney and Minghini, 2017; Yu and Gong,
2012) – as well as the rise of participatory research characterised by
greater user interactivity and collaboration, have increased the number of
studies and subjects investigated by citizen science projects. The use
of citizen science has also emerged in flood analysis in recent years. The
existing works can be classified according to which phase of flood risk
management they are dealing with, i.e. before, during or after the flood
event. For example, Sy et al. (2019a) reviewed the use of citizen science in
flood hazard assessments, discussing its potential to gather information
needed to develop realistic scenarios and provide flood hazard parameters,
such as extent and water depth, that could help understanding the hazard
level at a site. Assumpção et al. (2018) focused on the role citizen
science could play in flood modelling and demonstrated its value to provide
data for informing, calibrating and validating flood models, particularly
where data are scare. It is notable that most of the existing studies have
dealt with fluvial flooding; fewer studies have considered pluvial or
groundwater flooding (See, 2019). Moreover, none of those citizen science
projects have studied the reconstruction of past events using citizen
memory, unlike the field of wildlife conservation where Zhang et al. (2018)
demonstrated the value of citizen data for mapping past phenomena that were
not otherwise recorded.

The objective of this work is twofold: (1) retrieve flood extents and water
depths for different past events and (2) determine whether citizens can
clarify the causal chain of flood events. We also assessed the reliability
of these data by comparing them against independent methods, such as remote
sensing.

Our citizen science approach was applied to the suburbs of Yeumbeul North
(YN), one of the municipal districts of Pikine in Dakar, Senegal, western
Africa (Fig. 1). YN covers an area of about 9 km2. It is one of the
most populated districts of Senegal, with 168 379 inhabitants (ANDS, 2015)
and a population density of approximately 18 700 inhabitants km−2. YN is
characterised by lowlands with elevation less than 20 m above sea level and
is highly urbanised with more than 80 % of its territory covered with
buildings, critical facilities and roads (Sy et al., 2016). It is one of the
suburbs most affected by flooding. Figure 1 displays the state of the
permanent water bodies (Lake Warouwaye and Lake Wouye), which existed before
retention basins were implemented as a mitigation measure after the 2012
floods (GFDRR, 2014; Sy et al., 2016).

Figure 1Location of the study area. The insert on the right corner locates
our study area in the city of Dakar in Senegal. The central map represents
our study area Yeumbeul North without the retention basins that were
constructed after the 2012 flood. The 82 neighbourhoods are designated by a
number from 1 to 82. The corresponding names are provided in the
Supplement Table S1.

Administratively, YN is divided into 82 major neighbourhoods. In each of
these, a delegate, chosen among the inhabitants of the neighbourhoods,
represents the municipal administration (decree no. 86-761, Republic of Senegal, Republic of
Senegal) (GDS, 1986). The delegate should be from the neighbourhood and at
least 35 years old. One of the delegate's tasks is to inform the
neighbourhood inhabitants about how to face disasters. In this paper, we
refer to the delegate as a neighbourhood chief (NC; Tall, 1998), an appellation
employed by the local population.

Flooding in this area is mainly due to runoff and rainwater, which are not
absorbed by impermeable surfaces, made worse by rapid urbanisation and the
ineffective drainage network and combined with the rise of groundwater at some
locations. Therefore, our area is characterised by multiple types of floods.
Flooding occurs during the rainy season, which usually starts in July and
ends in October. The three events considered here occurred in 2005, 2009 and
2012. Their timeframe and the peak rainfall intensity are provided in Table 1. The timeframe was retrieved from the Emergency Events Database (EM-DAT,
2018), whereas the rainfall intensity values were registered at the station
of Dakar-Yoff, located 20 km away from the study area.

Table 1The beginning and the end of the three flood events according to the
Emergency Events Database (EM-DAT), as well as the rainfall intensity peak of
each event at the Dakar-Yoff station from the National Agency for Civil
Aviation and Meteorology (ANACIM) database in Senegal.

3.1 Investigation of past flood events

Since there is currently no catalogue of past flood events available for the
Dakar region, we decided to investigate the potential of citizen science in
the retrieval of this information. We developed a framework combining
different participatory approaches together in the field of citizen science
(Fig. 2).

The field campaign was carried out from July to August 2017. Our approach
involved two different groups of citizens. Participants were selected based
on three criteria: they (1) witnessed the three flood events, (2) have a good
spatial knowledge of both the study and flooded areas and (3) have a specific social
standing. Therefore, the first group consisted of the chiefs of the 82
neighbourhoods in the municipal district of YN. A chief is the qualification
given to an official delegate (Tall, 1986) representing the municipal
administration (GDS, 1986) and is therefore the focal point for the
inhabitants, also in case of disasters. The majority of this group was male
(98 %) and their ages varied from 40 to 90 years old, with an average of 66
years old. The second group was composed of 182 people, two or three per
neighbourhood. Of these, 72 % were men, with ages varying between 35 and 60. The
average was 38 years old. The underrepresentation of women in the study was
not by choice, but it is instead due to the sociocultural context of the country
(Creevey, 1996).

3.1.1 Neighbourhood chiefs: from episodic memory to flood information

For this group of citizens, we used a two-stage approach to optimise the
validity, reliability and utility of the data collected and to transform
memories of past floods into temporal and spatial information. The first
stage is based on the use of episodic memory through in-person interviews
conducted in the chief's house. Episodic memory is the process by which
humans remember events in context: date, place and emotional state (Tulving,
1972, 1993, 2002) and is part of long-term memory (Zacks et al., 2000). The
second stage involves participatory mapping (IFAD, 2009) and on-site visits.

Face-to-face interviews were conducted with each chief of the 82
neighbourhoods. These persons are nominated by the local population because
of their reputation, as they are considered senior and among the oldest
inhabitants of the neighbourhood. Each interview was expected to last
between 45 and 60 min, but it varied according to the narrative told, and
no time limit was imposed. Ultimately, interviews lasted from 30 to 60 min. In some cases it was possible to record the narrative digitally
using a smartphone. The information obtained from the narrative allowed the
neighbourhoods that were flooded to be identified. Then the chiefs of
flooded neighbourhoods were involved in participatory mapping in the house
and in the field, together with manual/GIS mapping for the latter case. The
purpose of this second step was to formalise and express the chiefs'
memories of the floods (as witnesses or victims) in an explicit form in order
to obtain past information useable for flood hazard assessment, such as
flood extent and water depth. Tools such as paper land-use maps of the area
with footprints of houses and different land-use categories (see Fig. 1), handheld GPS and mobile GIS, pins on the map were used.

Stage 1: Investigation of past flood information in the neighbourhood chief's house

The methodology of this stage was derived from techniques used in police
investigations (Fisher, 2010; Perfect et al., 2008). Compared to other forms
of interviews, it allows the witness (here the neighbourhood chief) to play
a more active role, by expressing freely their own narrative without being
interrupted or influenced by questions, which could distort the memory
(Loftus and Palmer, 1974). First, neighbourhood chiefs were put into a
relaxed state, allowing them to focus their thoughts and cognitive and
emotional states by closing their eyes (Perfect, 2008) and avoiding physical
and psychological distraction (e.g. telephone calls) during this phase, as
it requires intense concentration (Fisher, 2010). Some neighbourhood chiefs
felt uncomfortable when closing their eyes. In such cases, they were told to
focus on a blank surface, like a table or the floor. Once ready, they
expressed their memories of the event in the form of descriptive stories, as
they came to their mind, using their own words and language (Wolof) in order
to avoid misunderstandings. They were instructed to describe in detail
anything that may be related to the event, such as (a) processes that
accompanied the flood (e.g. the rupture of a water drainage pipe, man-made
obstacles); (b) important political or public events that could act as time
indicators (e.g. proximity to a presidential election, football game); (c) notable flood-related measures taken by the authorities enabling the event
to be dated; (d) spatial indicators such as place and street names allowing
reconstruction of the flooded areas; and (e) the event itself, including
information allowing for the deduction of the water depth (e.g. “the water reached
our knees”).

Following the narrative, only chiefs who indicated having been confronted
with floods went through participatory mapping using maps at the scale of
the neighbourhood (62 out of 82 chiefs, see Table S2). This
phase required training on how to read and use a map. Therefore, the
concerned neighbourhood chiefs were first familiarised with a land-use map
of their neighbourhood locating their house and other features in their area
including main and secondary roads as well as houses. After this
introductory explanation, the neighbourhood chiefs used the map to describe
their spatial perception of the different flood events, using a distinctive
colour pencil to draw the flood contours of each year. Coloured pins were
used for indicating the water depth at different locations on the map; red
for a high level of water, green for medium and yellow for low. This method
allowed a qualitative indication of the water depth as well as its spatial
distribution to be obtained.

Stage 2: Investigation of past flood information with neighbourhood chiefs in the field

The objective of stage 2 was to corroborate the chiefs' responses from stage
1 by cross-checking the information leading to the map from stage 1 with the
on-site mapping. To do this, neighbourhood chiefs brought us to the places
they previously described. This is important because memory retrieval is
facilitated when the context of the event is recreated, and neighbourhood
chiefs can also use their other senses (sight, hearing, smell) to better
remember the event (Rubin, 2005). We drew the polygon of the spatial extent
using a mobile GIS, with a GPS receiver automatically recording the site
location. Furthermore, we measured the water level as indicated by 49
neighbourhood chiefs with a graduated ruler (Tables S3, S4 and
S5) at 64 sites and recorded the GPS coordinates. Post-processing treatments
include merging the contours of flooded areas obtained on the paper map with
the ones obtained in the field as well as checking the correspondence
between qualitative water levels obtained with the coloured pins to the
quantitative water level measurements. The objective of the latter was to
verify if the sites indicated as having had very high water levels on the
paper map from stage 1 (red pin) corresponded to a high water level measured
in the field. Since we assume that memory retrieval is facilitated when one
is present at the site, we consider the field value to be more reliable.

3.1.2 Local representatives: participatory mapping on flood extent and water level of past flood events

The second group involved in investigating past flood events was composed of
182 people, selected by local associations (e.g. “Réseau d'Information
d'Education de Communication”, “Association des Relais Communautaires de
Yeumbeul”) that deal with the development of the neighbourhood and awareness of
health issues. The selection was based on the previously mentioned criteria.
As these associations operate locally, they personally know residents and
the choice of the inhabitants to be the representatives of the neighbourhood
was based on a consensus among the associations. From here on, we use the
term “local representatives” to refer to these selected people. The aim of
involving local representatives is to integrate their information with that
provided from the neighbourhood chiefs in order to check the consistency
between the two sources. Two or three local representatives were selected per
flooded neighbourhood, accounting for 130 out of 182 representatives, in
order for them to recall their memories and reach a common agreement
(Swanson et al., 2016) before providing information on flood extent and
water depths for the different flood events. Data on flood extent were
retrieved by participatory mapping using hands-on techniques. For this,
representatives were trained the same way as the chiefs. These maps were
then digitised. Regarding water level, local representatives went to the
same 64 sites as indicated by the chiefs; they did not have any prior
knowledge of the depths given by the chiefs, and depth information was given
using the different parts of the human body, e.g. ankle, knee or shoulder.
This strategy was proposed to provide local representatives with a visual
resource to describe the water level more easily. Then, the pre-defined tags
were converted into quantitative data by using average body segment lengths
expressed as a fraction of body height, as defined in the field of physical
anthropometry (Drillis and Contini, 1966; Winter, 2009). The bottom-up
dimensionless coefficients applied for each anthropometric segment
(Table S6) are (Winter, 2009; Contini, 1972) ankle (0.039),
knee (0. 285), wrist (0.485), elbow (0.63), chest (0.72), shoulder (0.818)
and chin (0.870). Finally, the water depth was obtained by multiplying the
value of the appropriate coefficient by the contributor's (local
representative; LR) height, as measured on site with a tape measure
(Tables S3, S4, S5 and S6). As we used two different approaches
to obtain the same information, we needed to assess the level of agreement
instead of the correlation between the two datasets. We used the
Bland–Altman method (1986), which determines the level of agreement between
data acquired with two different techniques, even if there is no information
about the “true” values (Bland and Altman, 1986). In our case, we assessed
depth values that could not be measured authoritatively during the flood
events under study. The Bland–Altman method calculates the differences
between the results obtained with two different approaches and plots them
against the average of the two approaches.

3.1.3 Remote sensing analysis

We used data from a remote sensing analysis to assess the reliability of the
extents of flooded areas provided by the two citizens groups. Our
requirements were (1) availability of images for the years considered, (2) free access to the data, (3) sufficient resolution for the size of our study area
(9 km2) and (4) minimum cloud cover. Radar images such as TerraSAR-X,
Radarsat-2 or COSMO-SkyMed can provide information with high resolution
(Schubert et al., 2012) and can capture flooded areas in cloudy conditions
at day and at night (Mason et al., 2014; Schumann and Moller, 2015), but they are not
free of charge, and, most importantly for our case, no images were available
for the periods of interest. Consequently, we only used available optical
satellite images from different sensors and from different sources. Indeed,
optical images were not available on Google Earth for the 2005 flood event.
The main characteristics of these products we used are given in Table 2.
Flooded areal extents were obtained following the process chain described in
Fig. 3.

For the 2005 event, we used two SPOT images (23 October) and (7 September) provided by
the applied Remote Sensing Laboratory (LTA) of the Institute of Earth
Sciences (IST) of the Université Cheikh Anta Diop (UCAD) (Table 2).

It should be noted that we did not find an image from before the flooding
and hence we used an image obtained during a dry period. These two
multispectral SPOT 5 images of 10 m resolution were merged with a SPOT 5
panchromatic image with a spatial resolution of 2.5 m to increase the
spatial accuracy. We then applied the normalised difference water index
(NDWI; Khajuria et al., 2017) to the water signature from other land-use
types. The NDWI is calculated following the method of McFeeters (1996),
using the green and the near-infrared (NIR) bands.

For the 2009 and 2012 events, we used images available from Google Earth.
Google launched Google Earth in 2005 (Cha and Pak, 2007), and it provides
free online aerial and satellite images covering many parts of the world,
with various resolutions and sensors. The highest resolution, about 0.5 m,
is provided by Worldwide and QuickBird satellite imagery operated by Digital
Globe. For each flood event, we examined the historical true colour
composite imagery from Google Earth using the time slider bar of Google to
find one image as close as possible to the flood event and another one in a
dry period after the event. These images were then photo-interpreted to
identify areas of water. These areas were digitised and then compared to
extract only areas considered as flooded.

4.1 Identifying the chain of events

The chain of events which triggered floods in YN was retrieved from the
narrative obtained from 82 neighbourhood chiefs. For the 2005, 2009 and 2012
events, all the 82 neighbourhood chiefs identified rainfall as the
primary factor. Of the 29 chiefs (neighbourhood numbers 1, 2, 3, 7, 9, 17, 19, 20,
28, 29, 31, 32, 33, 34, 35, 36, 39, 40, 41, 44, 49, 50, 56, 57, 62, 67, 70,
72, 76; see Fig. 1) also pointed out the rise of the water table,
substantiated by the wet ground, greening of walls due to the water
infiltration and removal of paint from walls.

The neighbourhood chiefs identified different processes that worsened the
flood, by either increasing the quantity of water or obstructing the typical
flow, for both different locations and events. For example, for the 2005
event, four neighbourhood chiefs (13, 36, 46, 67) mentioned the failure of
the pipeline in the road of Malika, used for water drainage, as increasing
the intensity of the flood event. Eight neighbourhood chiefs (7, 17, 18, 20, 21,
28, 45, 77) mentioned the overflow of Lake Warouwaye. Additionally, 15 neighbourhood
chiefs (7, 13, 17, 18, 19, 20, 21, 28, 36, 45, 46, 67, 72, 76, 77) mentioned
actions performed by the local population, such as the emptying of household
septic tanks, which aggravated this event and also had direct consequences
on health (e.g. cholera epidemics) (Wade et al., 2009). Pipeline failure
and the emptying of septic tanks also occurred during the 2009 event, but at
different locations, e.g. near the municipal hospital of YN for the
pipeline failure. For the 2012 event, the 82 chiefs did not recall any
processes that worsened the floods.

4.2 Flood extent mapping

Flood extents for the 2005, 2009 and 2012 events were obtained from the two
citizen groups using the methodologies described in Fig. 2 and then
compared to the results derived from the remote sensing analysis (Fig. 4).

Data obtained through the citizen science approach revealed that the 2005
event was the most widespread, whereas the 2012 event was the smallest (Table 3). Flooded areas provided by local representatives are slightly smaller
than those indicated by neighbourhood chiefs (Table 3), showing variations
from 1.8 % in to 2005 to 0.6 % in 2012 (Table 3).

Table 3Comparison of flooding areas from citizen science techniques
deployed in Yeumbeul North (neighbourhood chiefs and local representatives)
and remote sensing analyses.

In terms of mapping, slight differences appear between the extents
identified by the two citizen groups (Fig. 4), but the areas overlap
reasonably well (Fig. 5).

Figure 5Flooded areas obtained by the two citizen groups and remote
sensing with the surface of overlapping areas between the two results of the
citizen groups (orange), neighbourhood chiefs and remote sensing (dark blue), and local
representatives and remote sensing (purple).

The remote sensing analysis confirms that the main flooded areas were in the
central part of the study area (Fig. 4), but some discrepancies occur at the
edges. The total surface area is smaller than that provided by citizen
science for all years (Table 3), but it shows the same tendency of decreasing
surfaces from 2005 to 2012. We also find that flood extents provided by
neighbourhood chiefs agreed better with the remote sensing than those
provided by local representatives for all events.

4.3 Water depth information

Water depth is one of the key parameters considered in describing flood
intensity and mapping hazard (Van Alphen et al., 2007), but it is difficult to
record during flood events. Therefore, retrieving flood depths from past
events is of prime interest. Figure 6 displays scatter diagrams of depth
values obtained from the two different groups of citizens using the
techniques described in the methods (see Fig. 2) at 64 sites, sampled over
49 neighbourhoods. We have two measurements from each site. The maximum
retrieved flood depth is 2.5 m for the 2005 event, 1.5 m for the 2009 event
and 1.2 m for the 2012 event.

Figure 6Scatter diagram of water depth information provided by techniques
used with neighbourhood chiefs and local representatives for three different
flooding events in (a) 2005, (b) 2009 and (c) 2012.

Figure 7 shows the data obtained by applying the Bland–Altman method for the
2005, 2009 and 2012 events for the 64 measurement sites. The value of
the mean differences in water depth, indicated by the blue line, is 0.16 m
for the 2005 event, 0.23 m for 2009 and 0.26 m for 2012. The limits of
agreement, also displayed, are set at 95 % confidence intervals. Assuming
the differences are normally distributed, these limits are defined by the
mean difference ±1.96 multiplied by the standard deviation σ of
the differences. For the 2005 event, this range is from 0.68 to −0.37 m,
with two values falling outside these limits. For 2009 and 2012, three
values are outside the 95 % confidence interval which is from 0.78 to
−0.32 m for 2009 and 0.62 to −0.11 m for 2012.

In this study, we have used citizen science to retrieve information on three
past flood events that impacted the region of Dakar during the past 10 years. Our approach provides quantitative information on water depth, helps
retrieve the flood extents and provides insights into factors that aggravate
the intensity of floods.

Figure 7Bland–Altman plots for different flooding events in (a) 2005,
(b) 2009 and (c) 2012. These graphs show differences between water depth
provided by neighbourhood chiefs (NC) and local representatives (LR) in
metres against averaged values of NC and LR. Blue line is the mean
difference value, and the red dotted lines show the ±1.96
standard deviation (SD) water depth differences for all observations.

Our methodology consisted of a set of techniques designed to gather the most
complete spectrum of information. These techniques are unusual in the field
of flood hazard assessment, and we had to resolve some challenges associated
with the time that has elapsed since the events and participants'
understanding of maps. One technique is based on people's episodic memory;
we used face-to-face interviews with neighbourhood chiefs, applying specific
tools in order to limit external influence and memory distortion. The
procedure was then completed by a site visit with each neighbourhood chief
involved in order to consolidate the verbally provided information. The site
visit is very important because the time elapsed between the oldest event
and the date of this study is about 12 years. As time goes by, memories can
become vague (Lacy and Stark, 2013). However, people who have experienced
traumatic and stressful events, like floods, tend to retain a more accurate,
detailed and time-persistent memory of the event (Sotgiu and Galati, 2007).

Another technique involved participatory hands-on mapping. Mapping can
represent a challenging task for laypeople (Handmer, 1985; Żyszkowska,
2015, 2017), as they may have difficulties understanding and locating
themselves on a map. Moreover, maps are usually constructed by applying
standard rules of graphic semiology (Thomas, 2001) that does not necessary
take into account the cultural background or knowledge of the citizen (Fuchs
et al., 2009). Therefore, if a citizen has no experience in reading or
producing maps, information can be incorrectly reported. To overcome this
problem, we trained people on how to read a map and locate themselves to
ensure they understood the map, and we explained what they should be doing
and how to do it.

Developing the quality and reliability of citizen science data is a growing
research field (Crall et al., 2011; Flanagin and Metzger, 2008;
Silvertown et al., 2015). In our study, we developed different strategies in
order to improve these two aspects. We decided to work with two different
target groups according to the context and the purpose of the study. The
objective was to check the consistency of information obtained from the two
groups. If the same area is described as flooded by both groups, there is a
good chance that the area was indeed flooded. Due to the social organisation
of the Dakar region, we limited issues regarding source credibility
(Flanagin and Metzger, 2008) by involving neighbourhood chiefs. Indeed,
these chiefs are appointed by local citizens, according to the trust placed
in them and on their long-lasting presence in the area. Usually, they have a
good memory and good verbal abilities. Moreover, as a witness or sometimes
as a victim, they were at the forefront of the flood scene, therefore
representing a valuable source of information on the chain of events. The
second group was composed of local representatives, selected with the
support of local and well-implemented associations.

Identifying the chain of processes generating flooding is very important for
flood hazard assessment (DAEC, 2016) as it enables analysis of more
realistic flood scenarios. Citizens living in flood affected areas are not
frequently included in post-event or flood hazard assessments, even though
they could provide useful insights as they have a good understanding of
their surroundings (Tran et al., 2009) and in-depth local knowledge. Our
study demonstrates this as the neighbourhood chiefs identified both natural
and man-made factors that contributed to flooding, such as the rise of
ground water, the Lake Warouwaye overflow and the emptying of septic tanks.

In terms of flooded areas, the results obtained from the two groups of
citizens are similar for each event, although some spatial differences can
be observed regarding the extent. Reasons for the differences could be
related to (a) a more in-depth knowledge of the neighbourhood and their
surroundings by the chiefs, as they have the confidence (Tall, 1998) of the
inhabitants and therefore have access to more detailed information and (b) the
techniques used in mapping the areas. With neighbourhood chiefs, we used a
two-stage procedure to retrieve the flood extent, involving hands-on mapping
and GIS mapping in the field, whilst the local representatives only produced
hands-on maps that were then digitised.

A good spatial agreement exists between flood extents determined from remote
sensing and citizen science, with better agreement from the data provided by
the neighbourhood chiefs. However, areas provided by remote sensing are
smaller. This discrepancy can be explained by various factors. One could be
the different spatial resolutions of the selected images, which varied from
0.5 to 2.5 m; the larger were probably not being small enough to capture all
flooded areas (Grimaldi et al., 2016) at the scale at which we worked. A second
factor concerns the different time lapses between images. Post-event images
from Google Earth were captured at intervals from 1 to 15 d, and therefore they
may not have captured the maximum extent. Furthermore, for the 2005 event,
one image was obtained during the flooding, with the second image taken one
year after with the assumption it was captured during a dry period. A third
factor is related to technical limitations of the capability of optical
satellites to detect flooded areas, which is reduced when clouds are present
(Malinowski et al., 2017; Mallinis et al., 2013). A fourth factor could be
linked with the heterogeneity of sensors used in this study. A way to remove
this source of discrepancy would be to use satellite images obtained with
the same sensor. Finally, the efficiency of the NDWI index used to detect
water areas could be altered by noise (Xu, 2006).

One of the techniques used to retrieve water depths was inspired from
studies expressing flood hazard levels on maps using a body scale (e.g.
EXCIMAP, 2007; Luke et al., 2018). Therefore, quantitative data on water
depth were retrieved using a proportion of the size of the human body
borrowed from the field of physiology (Winter, 2009). These values represent
an average (Drillis and Contini, 1966), since the length of human body
segments depends on body structure (Contini, 1972), gender and racial groups, and therefore it could be a source of uncertainties. However, when
comparing the two approaches used for water depth investigation, we find a
fairly good agreement, with average differences less than 0.3 m, which is
within the range of other comparisons between observed and simulated methods
(Kutija et al., 2014).

Both involvement and motivation from citizens are necessary for the success
of citizen science projects (Rotman et al., 2012). As Facebook was one of
the most used social media in YN at the time of the study (Sy, 2019a), we
first created a page to interact with local citizens and motivate them to be
part of the project. Secondly, we designed and presented the project in a
way to convince contributors that their contribution will be beneficial for
them and their neighbours. Thirdly, we worked with community leaders
(Bénit-Gbaffou and Katsaura, 2014) and local associations to ensure a
better acceptance of the project.

Citizen science requires involvement and time, compared to a remote sensing
analysis which can now also take advantage of the free availability of radar
images such as Sentinel (Malenovský et al., 2012). However, at the scale
at which we worked, these images offer neither the required spatial resolution (Twele
et al., 2016) nor information on the depth of the flood, which is a
critical datum for flood hazard assessment that we were able to obtain with
citizen science.

In conclusion, our study shows the potential of citizen science in
retrieving quantitative and reliable information on past flood events,
especially in areas where no or few records of past events are available.
Our investigation strategy, involving two different groups of citizens,
increases the reliability of the obtained data. Provided that the
functioning of the society subject to floods is well understood, such an
approach can be replicated in other parts of the world. Moreover, the
citizens that have been involved in the various steps of this project have
developed skills in flood data acquisition and an understanding of flood
processes. They can thus better integrate into a decision-making process
regarding flood risk.

Raw Google images are accessible from the Google Earth portal. SPOT images are accessible on request to the owning institution, i.e. Institute of Science of Earth (IST) of the Université Cheikh Anta Diop in Dakar. All other related data are available at https://doi.org/10.26037/yareta:excgdpysdfadtcyffr4dclt3mm (Sy, 2019b).

BS conceived the study and carried out citizen science project in the field.
BS analysed the results and compiled the figures with input from CF. The
outline of the paper was drafted by BS, HD, DC, GG and CF. BS and CF
prepared the paper with contributions from all co-authors. All the
authors reviewed the paper.

The authors are grateful to Prof. Souleye Wade from the Applied Remote Sensing Laboratory
(LTA) of the Institute of Earth Sciences (IST) of the Université Cheikh Anta Diop in Dakar (UCAD) for providing them with the SPOT satellite images.

This field campaigns were supported by the Augustin Lombard grant from the Société de physique et d'histoire naturelle de Genève and Plantamour-Prévost grant from the Faculty of Science of the University of Geneva.

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